Eucrites

The Eucrites are named for a Greek word meaning "easily distinguished". Representing the most common class of achondrites, more than 100 eucrites are known, excluding all probable pairings. Although they are easily distinguished from chondrites, they closely resemble terrestrial basalts. Actually, eucrites are extraterrestrial basalts, volcanic rocks of magmatic origin, representing the crust of their parent body, Vesta. They are primarily composed of the calcium-poor pyroxene, pigeonite, and the calcium-rich plagioclase, anorthite. Additionally, eucrites often contain accessory minerals such as silica, chromite, troilite, and nickel-iron metal. Based on mineralogical and chemical differences, the eucrites have been further divided into three distinct subgroups: the non-cumulate group, the cumulate group, and the polymict group.

Camel Donga Found 1984, Western Australia TKW 25 kg Monolymict Eucrite
				Camel Donga -00 perfect individual with primary and secondary fusion crust 8.32gr $310
Camel Donga -01 superb oriented specimen with flow lines 8.06gr 320$
				Camel Donga -02 oriented specimen with bubbling....unfortunatly miss 30% 7.25gr$ $190
Camel Donga -03 nice complete elongated individual 5.89gr $220
				Camel Donga -04 complete individual 5.13gr $200
Camel Donga -05 90% crusted oriented flat stone 5.57gr $240
				Camel Donga -06 complete stone 4.96gr $210
Camel Donga -07 individual with primary and secondary fusion crust 4.73gr $200
				Camel Donga -08 very nice individual 4.69gr $200
Camel Donga -09 perfectly crusted stone 4.24gr $200
				Camel Donga -10 nice individual 4.21gr $160
Camel Donga -11 killer one !! 3.99 $180
				Camel Donga -12 nice complete stone 3.69gr $150